that includes the heterogeneity effects. Twice differentiating the result with respect to
and
and evaluating at the vertical reference (
and
), we arrive at the following layer traveltime derivatives:
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H![]() |
(15) |
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H![]() |
|
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H![]() |
denotes the traveltime of the
-th layer in the reference 1-D horizontally-layered anisotropic media with constant elastic parameters within each layer. Therefore, the terms with
derivatives are the usual results ones get under the 1-D medium assumption. The additional heterogeneous terms (H
) that combine the effects from curved interfaces and laterally varying velocity are given by
H![]() |
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(16) |
H![]() |
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|
H![]() |
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is similar to that of
with shifted indices. If a single horizontal layer is considered, equation 11 becomes reminiscent of the result by Grechka and Tsvankin (1999):
but with the second derivative on group slowness as opposed to group velocity.
is the usual normal-moveout velocity in the reference 1-D medium, which translates to
in the case of diffraction traveltime.